作为隐微修辞的“晚明”历史记忆——以《古今》杂志的“晚明”书写为中心

抗战时期,文人从"明清易代"的历史中找到熟悉的叙述和表达方式以言说自己的处境。作为一种"隐微修辞"策略,《古今》杂志文人通过言说"晚明"历史来阐扬心曲,塑造自身"遗民"的形象。通过考察以《古今》杂志为中心的文人对"晚明"的再叙述,可知"晚明记忆"成为沦陷区的文人曲折表达自己心声的历史资源。     

Late Mesozoic-Cenozoic décollement structure and its deep geological background in western Shandong,China

Data from seismic reflection profiles,drilling,stratigraphy,structural deformation studies and physical rock properties reveal the existence of drcollement structures in both shallow and deep levels in western Shandong,China.The most outstanding shallow décollement structures occur along the regional unconformity surface between the Cambrian and Archean,and the disconformity surface between the Carboniferous and Ordovician.The drcollement structure surface manifests as a fault zone with cataclastic rocks and asymmetrical folds.Some of the cataclastic rocks underwent dynamic metamorphism and hydrothermal alteration,including silicification,marbleization and specularite mineralization.Above the decollement structure,the bottom of the Cambrian might be missing or overprinted because of decollement.The striations,asymmetrical folds and boudinage structures indicate the direction of the main décollement tothe NNW and NNE.A deep level decollement structure occurs at a depth of 12-22 km and up to 30 km distance to the south.The early Cretaceous and Eocene are two main periods of activity,with the Cretaceous decollement probably initiated by mantle upwelling derived from subduction and collision of the Yangtze Plate with the North China Plate along the Tancheng-Lujiang Fault in the late Triassicearly Jurassic.This circumstance implies a multidirection of subduction and collision of these two plates in the early late Mesozoic.(C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences.Published by Elsevier Limited and Science in China Press.All rights reserved.     

内蒙古小孤山锡锌多金属矿的矿床地质特征与找矿意义

内蒙小孤山锡锌多金属矿是产于燕山期花岗斑岩与下二叠统大石寨组含碳质岩石接触带的热液成因矿床。该矿床没有地表露头．完全依靠大比例尺的地球化学土壤测量结合激电中梯、电阻率测量发现异常后进行钻探验证查明的。该矿床的查明为在大面积第四系覆盖区和地台区寻找隐伏矿体提供了有益帮助。     

鲁山籍总兵黄得魁事略

鲁山人黄得魁在咸丰八年（1858）至同治元年（1862）间,随胜保往返征战豫、皖、鲁、陕等省,屡立战功,官阶也不断提升。但因其靠山胜保被逮捕赐死,同治二年回籍养病后,黄得魁很快淡出清廷视线。     

女儿与父亲:受害者与施害者——《已故上校的女儿》浅析

本文就凯塞琳·曼斯菲尔所写的《已故上校的女儿》进行了浅析.着重分析了凯塞琳·曼斯菲尔笔下的父与女这种血缘关系实质上却是一种因长与囚犯,镇压者与被镇压者,施害者与受害者的关系。揭露了西方男性统治社会的腐败,号召妇女站立起来。     

贵州晚新生代矿产资源成因类型和成矿规律

本文将贵州晚新生代矿产资源分为沉积矿床和层控矿床二大成因类型。重点对层控矿床作了阐述,根据改造成矿作用程度和表生氧化成矿特点,进一步分为沉积——改造矿床、沉积——表生氧化矿床和沉积——改造——表生氧化矿床三类及若干亚类。并从成矿物质、成矿空间和成矿时间三个方面,对贵州晚新生代成矿规律作了探讨。其中,构造变异带成矿的规律至关重要。据此,对贵州晚新生代成矿区域作了划分;为成矿预测指明了方向。     

Speculation on the timing and nature of Late Pleistocene hunter－gatherer colonization of the Tibetan Plateau

1 Human biogeography on the edge The Qinghai-Tibetan Plateau occupies nearly 1.25 million km2 of the Asian continent and reaches an average elevation of more than 4000 m a.s.l. (Fig. 1). In addition to playing a critical role in global climate systems[1,2], the plateau is distinguished as the largest continuous high elevation ecosystem on the planet. This harsh, barren Fig. 1. Map of the Qinghai-Tibetan Plateau (left) and an elevation cross-section from the Badanjaran Desert in the n…     

Stephanorhinus kirchbergensis (Rhinocerotidae, Mammalia) from the Rhino Cave in Shennongjia, Hubei

The Rhino Cave,a Paleolithic site in Shennongjia,is the highest altitude locality of rhinoceros in the Middle-South part of China,and it is also the southernmost and the richest locality in Stephanorhinus kirchbergensis fossils which include cranium,mandibles,isolated teeth and postcranials.These materials can be referred to the species Stephanorhinus kirchbergensis according to the following characters:incisorless,mandibular symphysis contracted,occiput high,subaural channel closed,with nasal and frontal h...     

《晚清民国湖湘词坛研究》评析

《晚清民国湖湘词坛研究》是系统研究湖南地域词学的首部学术专著,其筚路蓝缕之功不待多言。这部著作突出的特点有三：一是自觉的文学史意识,包括纵向的湖南词学史与横向的晚清民国词学史意识;二是多元的研究方法,包括定量的表格分析、细致的文献考证、透彻的理论分析;三是扎实的研究内容,包括词学思想与词家词作的研究。